祁连山北坡不同纬度青海云杉及林下土壤化学计量特征研究
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1.西北师范大学地理与环境科学学院;2.甘肃省国家公园监测中心

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基金项目:

国家自然科学基金资助项目(面上项目,重点项目,重大项目);祁连山国家公园甘肃片区定位监测体系基础数据库建设项目


Characterization of Qinghai spruce and understory soil chemometrics at different latitudes on the northern slopes of Qilian Mountains
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College of Geography and Environmental Science, Northwest Normal University

Fund Project:

The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan);Qilian Mountains National Park Gansu Area Positioning Monitoring System Basic Database Construction Project

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    摘要:

    深入探讨植物和土壤化学计量的空间格局和驱动因子,对于把握元素循环和量化生态系统对环境因子的响应具有重要意义。基于此,实验测定了祁连山北坡不同纬度青海云杉组织及土壤碳(C)氮(N)磷(P)含量,采用单因素方差分析(One-Way ANOVA)、皮尔逊相关分析(Pearson correlation)及冗余分析(Redundancy analysis,RDA)来揭示祁连山北坡不同纬度青海云杉及林下土壤化学计量特征及关键影响因素。结果表明:(1)青海云杉组织和土壤C、N含量随纬度增加而减少;而青海云杉组织N:P、C:P随纬度增加而增大,土壤N:P、C:P则减小。(2)青海云杉组织养分分配不均衡,C、N元素含量,叶>枝>根,而P元素含量,枝>叶>根,且青海云杉枝、根N:P均小于14,表明祁连山青海云杉生长受土壤N元素的限制。(3)土壤因子(含水量、pH值、容重、SOC、TN、TP及SOC:TN:TP)及气候因子(年均气温和年均降水量)变化影响青海云杉组织N、P元素含量,且土壤因子对植物组织N、P、N:P的解释率大于气候因子,其中,植物叶片N、N:P与土壤TN、TN:TP呈正相关(P<0.05),而植物根系N、N:P值与气温呈负相关、与年均降水量呈显著正相关(P<0.05)。本研究有助于评估祁连山青海云杉生态系统养分动态变化,探索不同纬度青海云杉林养分调控分配机理,以期为祁连山森林生态系统的持续健康发展提供科学依据。

    Abstract:

    An in-depth exploration of the spatial patterns and drivers of plant and soil stoichiometry is important for grasping elemental cycling and quantifying ecosystem responses to environmental factors. This paper experimentally determined the carbon (C), nitrogen (N) and phosphorus (P) contents of Qinghai spruce tissues and soils at different latitudes on the northern slopes of the Qilian Mountains. One-way ANOVA, Pearson correlation, and redundancy analysis were used to reveal the stoichiometric characteristics and key influencing factors of Qinghai spruce and understorey soils at different latitudes on the northern slopes of the Qilian Mountains. The results showed that: (1) the C and N contents of the Qinghai spruce tissues and soils decreased with the increasing latitude; whereas the N:P and C:P of the Qinghai spruce tissues increased with the increasing latitude, and the N:P and C:P of the soils decreased. (2) The nutrient distribution of Qinghai spruce tissues was unbalanced, with the content of C and N elements in the order of leaves>branches>roots, and the content of P elements in the order of branches>leaves>roots, and the N:P of Qinghai spruce branches and roots being less than 14, which indicated that the growth of Qinghai spruce in Qilian Mountains was limited by soil N element. (3) Changes in soil factors (water content, pH, bulk weight, SOC, TN, TP and SOC:TN:TP) and climatic factors (mean annual temperature and mean annual precipitation) affected the elemental content of N and P in Qinghai spruce tissues. The soil factors explained more of the N, P, and N:P of plant tissues than did the climatic factors, in which, the plant leaf N and N:P were positively correlated with soil TN and TN:TP ( P<0.05), while plant root N, N:P values were negatively correlated with temperature and significantly positively correlated with mean annual precipitation (P<0.05). The study helps to assess the plant-soil nutrient dynamics of Qinghai spruce ecosystems in the Qilian Mountains, and explore the mechanism of nutrient regulation and allocation in Qinghai spruce forests at different latitudes, with a view to providing a scientific basis for the sustained and healthy development of forest ecosystems in the Qilian Mountains.

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武锦艳,张 华,李兴民.祁连山北坡不同纬度青海云杉及林下土壤化学计量特征研究.生态学报,,(). http://dx. doi. org/[doi]

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